CO ho co h


GeH4 + H2S ^ GeS(s) + 3H2 4PH3 + 6H20 ^ P406 + 12H2 4AsH3 ^ As4(s) + 6H2

Measurements of the vertical profiles of these species provide constraints in the eddy-mixing coefficient as mentioned earlier. Mapping the spatial abundance of these materials provides information on the general upwelling/downwelling motions.

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